Frontal Convergence
Frontal Convergence is a physical oceanographic phenomenon characterized by the horizontal coming together of distinct water masses at an oceanic front, resulting in the net accumulation of fluid properties and enhanced vertical motion due to differential buoyancy and dynamic forcing.
28
Publications
1.2K
Citations
91
Authors
54
Institutions
Publications per year
2017–2026
6
Parents
28
1–5 of 28
91
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University of California, Los Angeles, United States
2 publications · 56 citations
2
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1
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1–5 of 91
54
Woods Hole Oceanographic Institution
Falmouth, United States
3 h-index
6 publications
340 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
3 h-index
9 publications
213 citations
University of California, Los Angeles
Los Angeles, United States
3 h-index
10 publications
220 citations
The University of Tokyo
Tokyo, Japan
2 h-index
5 publications
215 citations
Nagoya University
Nagoya, Japan
2 h-index
6 publications
150 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
2 h-index
6 publications
162 citations
University of California San Diego
San Diego, United States
2 h-index
3 publications
124 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
3 publications
124 citations
1–8 of 54
5 publications · 169 citations
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JGR · 4 publications · 194 citations
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3 publications · 169 citations
3
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2 publications · 56 citations
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2 publications · 41 citations
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1–5